Abstract
The free convection boundary-layer flow of a Darcy–Boussinesq fluid from a vertical permeable plate with an inverse-linear temperature distribution is considered. The outstanding characteristics of this self-similar flow which, according to the usual reduction procedure of pseudo-similarity to full similarity, should not exist at all, are analyzed in detail. Thus it is shown that this flow only exists if a lateral suction with a sufficiently large suction parameter γ ≥ γmin = 1.079131 is applied. For the threshold value γmin the solution is unique but above it multiple solutions are encountered for every given value of γ.
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Magyari, E., Pop, I. & Keller, B. The ‘Missing’ Self-Similar Free Convection Boundary-Layer Flow Over a Vertical Permeable Surface in a Porous Medium. Transport in Porous Media 46, 91–102 (2002). https://doi.org/10.1023/A:1013816831733
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DOI: https://doi.org/10.1023/A:1013816831733